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  • Letter

Spontaneous generation and reversal of helicity in anisotropic turbulence

Wesley Agoua*

Benjamin Favier

Alexandre Delache

Antoine Briard

Wouter J. T. Bos†

  • CNRS, Univ Lyon, Ecole Centrale de Lyon, Univ Lyon 1 Claude Bernard, INSA Lyon, Laboratoire de Mécanique des Fluides et d'Acoustique, UMR5509, 69134 Ecully, France

  • Aix Marseille Univ, CNRS, Centrale Marseille, IRPHE UMR 7342, Marseille, France

  • CNRS, Univ Lyon, Ecole Centrale de Lyon, Univ Lyon 1 Claude Bernard, INSA Lyon, Laboratoire de Mécanique des Fluides et d'Acoustique, UMR5509, 69134 Ecully, France and Université Jean Monnet de Saint Etienne, 42000 Saint Etienne, France

  • CEA, DAM, DIF, F-91279 Arpajon, France

  • CNRS, Univ Lyon, Ecole Centrale de Lyon, Univ Lyon 1 Claude Bernard, INSA Lyon, Laboratoire de Mécanique des Fluides et d'Acoustique, UMR5509, 69134 Ecully, France

  • *wesley.agoua@ec-lyon.fr.
  • †wouter.bos@ec-lyon.fr

Phys. Rev. E 103, L061101 – Published 8 June, 2021

DOI: https://doi.org/10.1103/PhysRevE.103.L061101

Abstract

Helicity plays an important role in spectacular geophysical phenomena such as hurricanes or the generation of the terrestrial magnetic field. The present investigation shows how helicity can be created in a statistically homogeneous but anisotropic flow, driven by buoyancy. If the flow is close enough to a two-dimensional limit, spontaneous symmetry breaking leads to the generation of mean helicity. In particular, we explain these observations by identifying a simple linear mechanism, the relevance of which is illustrated by simulations of unstably stratified turbulence in a conducting fluid on which a magnetic field is imposed. Finally it is shown that the self-organized state displays dynamical reversals of the sign of the mean helicity.

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